Geologic factors in the Basin and Range province in Utah are more favorable for the occurrence of geothermal resources than in other areas on the Colorado Plateaus or in the Middle Rocky Mountains. These geologic factors are principally crustal extension and crustal thinning during the last 17 million years. Basalts as young as 10,000 years have been mapped in the area. High-silica volcanic and intrusive rocks of Quaternary age can be used to locate hydrothermal convection systems. Drilling for hot, high-silica, buried rock bodies is most promising in the areas of recent volcanic activity. Southwestern Utah has more geothermal potential than other parts of the Basin and Range province in Utah. The Roosevelt Hot Springs area, the Cove Fort-Sulphurdale area, and the area to the north as far as 60 kilometers from them probably have the best potential for geothermal development for generation of electricity. Other areas with estimated reservoir temperatures greater than 150°C are Thermo, Monroe, Red Hill (in the Monroe-Joseph Known Geothermal Resource Area), Joseph Hot Springs, and the Newcastle area. The rates of heat and water discharge are high at Crater, Meadow, and Hatton Hot Springs, but estimated reservoir temperatures there are less than 150°C. Additional exploration is needed to define the potential in three additional areas in the Escalante Desert.
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Oklahoma: U.S. Geological Survey Open-File Report 83-115, maps :photocopy ;45 x 75 cm., https://doi.org/10.3133/ofr83115.","productDescription":"maps :photocopy ;45 x 75 cm.","costCenters":[],"links":[{"id":169244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af06d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43919,"text":"ofr83112 - 1983 - Land use and land cover and associated maps for Sheridan, Wyoming; Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr83112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-112","title":"Land use and land cover and associated maps for Sheridan, Wyoming; Montana","language":"ENGLISH","doi":"10.3133/ofr83112","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Sheridan, Wyoming; Montana: U.S. Geological Survey Open-File Report 83-112, maps :photocopy ;45 x 70 cm., on sheet 77 x 107 cm., https://doi.org/10.3133/ofr83112.","productDescription":"maps :photocopy ;45 x 70 cm., on sheet 77 x 107 cm.","costCenters":[],"links":[{"id":169243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af1d3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43169,"text":"ofr83572 - 1983 - Land Use Series, Casper [Quadrangle], Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:10","indexId":"ofr83572","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-572","title":"Land Use Series, Casper [Quadrangle], Wyoming","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr83572","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land Use Series, Casper [Quadrangle], Wyoming: U.S. Geological Survey Open-File Report 83-572, Maps, https://doi.org/10.3133/ofr83572.","productDescription":"Maps","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":176395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108,42 ], [ -108,43 ], [ -106,43 ], [ -106,42 ], [ -108,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b41fa","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531006,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19761,"text":"ofr83842 - 1983 - A computer program written in HPL for acquisition and reduction of stable isotope data using a Hewlett Packard 9825A desktop computer","interactions":[],"lastModifiedDate":"2012-02-02T00:07:49","indexId":"ofr83842","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-842","title":"A computer program written in HPL for acquisition and reduction of stable isotope data using a Hewlett Packard 9825A desktop computer","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83842","usgsCitation":"Landis, G.P., 1983, A computer program written in HPL for acquisition and reduction of stable isotope data using a Hewlett Packard 9825A desktop computer: U.S. Geological Survey Open-File Report 83-842, i, 39 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83842.","productDescription":"i, 39 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0842/report-thumb.jpg"},{"id":49233,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0842/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0985","contributors":{"authors":[{"text":"Landis, G. P.","contributorId":102846,"corporation":false,"usgs":true,"family":"Landis","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":181461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19423,"text":"ofr83774 - 1983 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","interactions":[{"subject":{"id":19423,"text":"ofr83774 - 1983 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"ofr83774","publicationYear":"1983","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"wsp2258","publicationYear":"1985","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"id":1}],"supersededBy":{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"wsp2258","publicationYear":"1985","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"lastModifiedDate":"2021-01-26T19:53:48.989552","indexId":"ofr83774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-774","title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","docAbstract":"The Papago Farms-Great Plain and upper Rio Sonoyta study area includes about 490 square miles in south-central Arizona and north-central Sonora, Mexico. In the study area 23,700 acre-feet of ground water from the basin-fill deposits was used to irrigate more than 5,000 acres in 1981. Surface water is not a reliable source for irrigation or public supply. Ground water enters the area as underflow from the north and east and as recharge from the mountains, moves through basin-margin sediments, around the basin-center clays, and exits the area to the west beneath the Rio Sonoyta. Ground-water withdrawals in the upper Rio Sonoyta area do not appear to have an effect on water levels in the Papago Farms-Great Plain area. Depth to water ranges from 500 feet near the southern boundary to 150 feet in the center of study area. About 10 million acre-feet of recoverable ground water is stored in the upper 400 feet of the aquifer. Storage is being depleted at a rate of 19,000 acre-feet per year. The ground water is a sodium and bicarbonate type and has an anomalously high content of arsenic and fluoride. (USGS)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83774","usgsCitation":"Hollett, K., 1983, Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico: U.S. Geological Survey Open-File Report 83-774, vi, 76 p., https://doi.org/10.3133/ofr83774.","productDescription":"vi, 76 p.","costCenters":[],"links":[{"id":382608,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0774/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Papago Indian Reservation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.2470703125,\n 31.765537409484374\n ],\n [\n -111.236572265625,\n 31.765537409484374\n ],\n [\n -111.236572265625,\n 33.0178760185549\n ],\n [\n -113.2470703125,\n 33.0178760185549\n ],\n [\n -113.2470703125,\n 31.765537409484374\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b25","contributors":{"authors":[{"text":"Hollett, K.J.","contributorId":23570,"corporation":false,"usgs":true,"family":"Hollett","given":"K.J.","affiliations":[],"preferred":false,"id":180879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19670,"text":"ofr83815 - 1983 - Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data","interactions":[],"lastModifiedDate":"2022-09-01T21:00:22.928432","indexId":"ofr83815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-815","title":"Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data","docAbstract":"Electromagnetic induction data using distant field sources, mostly of natural origin, in the frequency range of 4.5-27,000 Hz are analyzed to depict the geoelectric structure in an area of volcanic-rock cover located in southeastern Arizona between the Morenci and Safford porphyry copper deposits. The data for each station consist of scalar electromagnetic measurements at descrete frequencies for two-orthogonal magnetic and electric field pairs. Observations spaced about 5-km apart indicate resistivities in the range of 100-700 ohm-m for the unweathered Tertiary volcanic rocks to a depth of 200 to 500 m. Beneath this zone the data indicate resistivities in the range of 10-100 ohm-m that suggest the existence of an older volcanic rock unit. The less resistive unit appears to be displaced upward beneath Turtle Mountain, an area bounded to the northeast and southwest by mapped Basin and Range faults, and bounded to the southeast by an unmapped fault of older origin that trends northeast. Lateral changes in the resistivity of the two main geoelectric layers result in lowered resistivity in an area of known hot-springs near the confluence of the Gila and San Francisco Rivers, as well as along a north-south trending zone located on the east flank of Turtle Mountain, about 5-km (3-mi) west-northwest of the hot springs. This second anomaly is at a probable depth of 400-500 m and is interpreted to indicate a buried fault or fracture zone.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83815","usgsCitation":"Klein, D.P., and Baer, M.J., 1983, Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data: U.S. Geological Survey Open-File Report 83-815, 109 p., https://doi.org/10.3133/ofr83815.","productDescription":"109 p.","costCenters":[],"links":[{"id":406098,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14236.htm","linkFileType":{"id":5,"text":"html"}},{"id":49135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0815/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0815/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Graham County, Greenlee County","otherGeospatial":"Gila-San Francisco Wilderness Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.566,\n 33.076\n ],\n [\n -109.32,\n 33.076\n ],\n [\n -109.32,\n 32.833\n ],\n [\n -109.566,\n 32.833\n ],\n [\n -109.566,\n 33.076\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9b4e","contributors":{"authors":[{"text":"Klein, D. 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J.","contributorId":102487,"corporation":false,"usgs":true,"family":"Baer","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":181309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19447,"text":"ofr83622 - 1983 - Audio-magnetotelluric and telluric data release for the Ten-Lakes Wilderness study area, Montana","interactions":[],"lastModifiedDate":"2021-10-27T19:45:18.040555","indexId":"ofr83622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-622","title":"Audio-magnetotelluric and telluric data release for the Ten-Lakes Wilderness study area, Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83622","usgsCitation":"Hoover, D., and Broker, M., 1983, Audio-magnetotelluric and telluric data release for the Ten-Lakes Wilderness study area, Montana: U.S. Geological Survey Open-File Report 83-622, 51 p., https://doi.org/10.3133/ofr83622.","productDescription":"51 p.","costCenters":[],"links":[{"id":391032,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14138.htm"},{"id":48923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0622/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0622/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Ten-Lakes Wilderness study area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.95,\n 48.9\n ],\n [\n -114.9670,\n 48.9\n ],\n [\n -114.9670,\n 48.925\n ],\n [\n -114.95,\n 48.925\n ],\n [\n -114.95,\n 48.9\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66934a","contributors":{"authors":[{"text":"Hoover, D.B.","contributorId":37734,"corporation":false,"usgs":true,"family":"Hoover","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":180922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broker, M. 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